Carbokentbrooksite | |
Category: | Silicate mineral, Cyclosilicate |
Formula: | (Na,□)12(Na,Ce)3Ca6Mn3Zr3Nb(Si25O73)(OH)3(CO3)·H2O (original form) |
Imasymbol: | Cktb[1] |
Strunz: | 9.CO.10 (10 ed) 8/E.25-32 (8 ed) |
Dana: | 64.1.2.3 |
Class: | Ditrigonal pyramidal (3m) (same H-M symbol) |
Symmetry: | R3m |
Unit Cell: | a = 14.24, c = 30.04 [Å]; Z = 3 |
Color: | Yellow, yellow-orange |
Habit: | rhombohedra (cores of zoned crystals) |
Cleavage: | None |
Fracture: | Conchoidal |
Tenacity: | Brittle |
Mohs: | 5 |
Luster: | Vitreous |
Streak: | White |
Diaphaneity: | Transparent |
Density: | 3.14 (measured) |
Opticalprop: | Uniaxial (−) |
Refractive: | nω = 1.65, nε = 1.64 (approximated) |
Pleochroism: | None |
Fluorescence: | No |
Carbokentbrooksite is a very rare mineral of the eudialyte group,[2] with formula (Na,□)12(Na,Ce)3Ca6Mn3Zr3NbSiO(Si9O27)2(Si3O9)2(OH)3(CO3).H2O.[3] The original formula was extended to show the presence of cyclic silicate groups and silicon at the M4 site, according to the nomenclature of eudialyte group.[4] Carbokenbrooksite characterizes in being carbonate-rich (the other eudialyte-group species with essential carbonate are zirsilite-(Ce), golyshevite, and mogovidite). It is also sodium rich, being sodium equivalent of zirsilite-(Ce), with which it is intimately associated.
Carbokentbrooksite and zirsilite-(Ce) are found as replacements of grains and crystals of eudialyte. They occur in pegmatites of Darai-Pioz alkaline massif, Tajikistan – a locality known for many rare minerals.[5] The minerals are associated with aegirine, ekanite, microcline, polylithionite, quartz, stillwellite-(Ce) (silicates), pyrochlore-group mineral, fluorite, calcite, and galena.
Beside the elements given in the formula, carbokentbrooksite contains admixtures of lanthanum, strontium, neodymium, iron, yttrium, titanium, potassium, chlorine, and praseodymium. Carbokentbrooksite and zirsilite-(Ce) are chemically similar.
Carbokentbrooksite is isostructural with kentbrooksite.